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Glaciers of the Orulgan Range: assessment of the current state and possible development for the middle of the 21st century

机译:Orulgan山脉冰川:对21世纪中叶的现状和可能发展的评估

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An assessment of the current state of Orulgan Range (part of Verkhoyansky Range, the NE Siberia) glaciers is proposed. It was conducted involving ASTER images for the summer 2010 and the corresponding DEM. We have identified 70 % of the glaciers, outlined in the Inventory of glaciers of the USSR, Part. 2. Orulgan range. Leningrad: Hydrometeoizdat 17(5): 67, (1972). The mean relative degree of the area reduction for Orulgan glaciers is about 60 % from that time up to 2010. Using ASTER GDEM, the equilibrium line altitudes were defined for contemporary glacier systems of the Orulgan. We used climatic scenario for the period 2049-2060, which is an addition to the global temperature of 1.5 degrees (the array developed by Institute of Global Climate and Ecology, RAS) and corresponding to this increase precipitation-the array of Voeikov Observatory, Sankt-Peterburg, identified by 31 AOGCMs (involved in the CMIP5 project), in particular, RCP4.5 to project the glacier development to 2049-2060. The previously developed technique used the outputs for assessing the evolution of the Orulgan glacier systems. Results showed that under the scenario combination of precipitation, feeding glaciers, and summer temperatures, the Orulgan glaciation actually would disappear. These results are compared with the earlier projection made involving the ECHAM 4 as a climate scenario (Ananicheva et al., Cryosphere 4: 435-445, 2010).
机译:提出了对Orulgan山脉(东北西伯利亚Verkhoyansky山脉的一部分)冰川当前状态的评估。进行了涉及2010年夏季的ASTER图像和相应的DEM。我们已经确定了70%的冰川,这在《苏联冰川清单》中有概述。 2. Orulgan系列。列宁格勒:Hydrometeoizdat 17(5):67,(1972)。从那时到2010年,Orulgan冰川的平均面积缩小程度约为60%。使用ASTER GDEM,可以为Orulgan当代冰川系统定义平衡线高度。我们使用了2049-2060年期间的气候情景,这是对全球温度1.5度(由RAS全球气候与生态研究所开发的阵列)的补充,并且与这种增加的降水量相对应-Sankt Voeikov天文台的阵列-彼得堡,由31个AOGCM(参与CMIP5项目)确定,特别是RCP4.5,将冰川发展预测到2049-2060年。先前开发的技术使用输出评估Orulgan冰川系统的演化。结果表明,在降水,冰川进食和夏季温度共同作用下,Orulgan的冰川作用实际上将消失。将这些结果与早期将ECHAM 4作为气候情景的预测进行了比较(Ananicheva等人,Cryosphere 4:435-445,2010)。

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